Azincourt Energy Corp. announced that the sample analysis has finally been received from the 2023 exploration program at the East Preston uranium project in the Athabasca Basin, Saskatchewan, Canada. Drilling for the 2023 program at the East Preston Project consisted of a total of 3,066 meters completed in 13 drill holes between February and March 2023.

Drilling was focused on the G, K, H, and Q zones with results reported in a news release dated March 28th, 2023. Winter 2023 Diamond Drilling Program Highlights: A total of 687 samples were collected throughout the program and sent to the Geoanalytical Laboratory at the Saskatchewan Research Council in Saskatoon, Saskatchewan for analysis. As was reported in a news release dated July 11, 2023, there was a delay with the analytical results.

After a review of the initial data received from the lab, there were significant quality control issues noted within the results. As part of the quality control process, standards with a known concentration of uranium are inserted in the sample batches. These samples are analyzed to confirm that the results for that batch of samples are within an acceptable range based on the results of the standards.

The issues noticed manifested as anomalous results occurring in the samples analyzed immediately following several of the standards. As a result, these samples were reanalyzed. Once the issue was identified, confirmed, and resolved, the company requested that all samples of the affected batches be run through the process to ensure a complete consistent data set.

Analysis of the results shows uranium enrichment within the previously identified clay alteration zones along the K, and H- target zones. Uranium enrichment is identified as uranium (U) values and a uranium/thorium ratio (U/Th) above what would normally be expected in the given rock type or area. Drilling on the northeast trending G-Zone identified extensive hydrothermal alteration and evidence of east-west cross-cutting structures along the southern portion of the zone.

The primary rock types in the alteration zone are granodiorite and diorite gneiss with average expected values of 2-3 ppm U and U/Th ratios of 0.25-0.3. Elevated radioactivity was intersected in EP0045 and EP0047 and EP0047 returned elevated U and U/Th values. While this is a good sign, the alteration zone does not display the upgraded clay alteration halo seen at Zones K and H. Illite and kaolinite are both indicators of hydrothermal alteration typically found within alteration halos of unconformity uranium deposits. Dravite is a boron-rich clay which is typically found within a larger clay package in close proximity to uranium mineralization in the system.

Both illite and dravite have been identified as being significant vectors for the recent Patterson Lake North discovery by F3 Uranium approximately 60 km to the northwest of the East Preston project. On the north end of the K-Zone, drilling intersected extensive structure and hydrothermal clay alteration within the structural zone. Samples of clay alteration were analyzed by Short Wavelength Infrared Reflectance (SWIR, sometimes referred to as ?PIMA?) to confirm the clay species.

All three holes contained illite and kaolinite clay species, with EP0049 also having dravite identified within the structural zone. EP0049 also returned elevated Thorium. The H-Zone covers a change in orientation of the structural and conductive trend from north south to southwest trending.

Drilling intersected an intense graphitic fault zone with hydrothermal alteration. The Illite clay alteration halo identified in the K-Zone extends south into the H Zone as far south as EP0053. Hole EP0053 intersected elevated radioactivity and both kaolinite and dravite are also present within the illite alteration package.

Dravite was also identified in hole EP0052. Rocks in this zone are expected to return values of 0.5-1.5 ppm U and U/Th ratios of 0.25-0.5. Holes EP0052 and EP0056 returned the best analytical results of the program with U/Th ratios of 1.0 and 1.8 respectively, and uranium in the 5-6 ppm range. The company considers the drilling results to date to be significant, as major uranium discoveries in the Athabasca Basin such as McArthur River, Key Lake, and Millennium were primarily the result of drill testing of strong alteration zones related to conductor features.

Identifying and upgrading the strong alteration zones is a significant step forward in identifying the key areas along the conductor trends where more attention is required. The primary target area on the East Preston Project is the conductive corridors from the A-Zone through to the G-Zone (A-G Trend) and the K-Zone through to the H and Q-Zones (K-H-Q Trend). The selection of these trends is based on a compilation of results from the 2018 through 2020 ground-based EM and gravity surveys, property wide VTEM and magnetic surveys, and the 2019 through 2022 drill programs, the 2020 HLEM survey indicates multiple prospective conductors and structural complexity along these corridors.

Drilling has confirmed that identified geophysical conductors comprise structurally disrupted zones that are host to accumulations of graphite, sulphides, and carbonates. Hydrothermal alteration, anomalous radioactivity, and elevated uranium have been demonstrated to exist within these structurally disrupted conductor zones. The permitting process is underway for the 2024-2026 drill programs. Azincourt Energy continues to be engaged in regular meetings with the Clearwater River Dene Nation and other rights holders to ensure that concerns of the local communities are addressed with regards to the East Preston project.

A more in-depth engagement process will also be commencing within the next couple of months with the La Loche Metis Local #39. Azincourt looks forward to a continued close working relationship with CRDN and other rights holders to ensure that any potential impacts and concerns are addressed and that the communities can benefit from activities in the area through support of local business, employment opportunities, and sponsorship of select community programs and initiatives. Local businesses are engaged to provide services and supplies and members of the Clearwater River Dene Nation and surrounding communities have been directly employed on site or to provide support and services to keep the camp and programs running.